Sequence stratigraphy and inferred relative sea-level change from the onshore British Jurassic

Sequence stratigraphy - the subdivision of successions into facies packages bounded by surfaces representing major shifts in depositional environment - has provided a systematic methodology for inference of relative sea-level change from vertical facies successions. In the present review, sequence s...

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Main Author: Hesselbo, S
Format: Journal article
Language:English
Published: 2008
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author Hesselbo, S
author_facet Hesselbo, S
author_sort Hesselbo, S
collection OXFORD
description Sequence stratigraphy - the subdivision of successions into facies packages bounded by surfaces representing major shifts in depositional environment - has provided a systematic methodology for inference of relative sea-level change from vertical facies successions. In the present review, sequence stratigraphic work on exposures of British Jurassic successions is summarized. Resultant inferred relative sea-level curves for Early Jurassic and early Mid Jurassic successions show some strong similarities at the scale of ammonite zones between widely separated basins, implying sea-level change of at least regional extent or, alternatively, regionally co-ordinated changes in sediment supply. Also well developed are coeval stage-level influxes of sandy sediments into widely separated marine basins during the Late Pliensbachian, Late Toarcian-Aalenian and Oxfordian. Similarly, widespread synchronous shifts to more offshore facies are evident in the Early Pliensbachian, Early Toarcian, Early Callovian and Early Kimmeridgian. © 2008 Geologists' Association.
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spelling oxford-uuid:3d07555d-5461-49ad-b015-aef2a4dbbe9c2022-03-26T14:17:13ZSequence stratigraphy and inferred relative sea-level change from the onshore British JurassicJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:3d07555d-5461-49ad-b015-aef2a4dbbe9cEnglishSymplectic Elements at Oxford2008Hesselbo, SSequence stratigraphy - the subdivision of successions into facies packages bounded by surfaces representing major shifts in depositional environment - has provided a systematic methodology for inference of relative sea-level change from vertical facies successions. In the present review, sequence stratigraphic work on exposures of British Jurassic successions is summarized. Resultant inferred relative sea-level curves for Early Jurassic and early Mid Jurassic successions show some strong similarities at the scale of ammonite zones between widely separated basins, implying sea-level change of at least regional extent or, alternatively, regionally co-ordinated changes in sediment supply. Also well developed are coeval stage-level influxes of sandy sediments into widely separated marine basins during the Late Pliensbachian, Late Toarcian-Aalenian and Oxfordian. Similarly, widespread synchronous shifts to more offshore facies are evident in the Early Pliensbachian, Early Toarcian, Early Callovian and Early Kimmeridgian. © 2008 Geologists' Association.
spellingShingle Hesselbo, S
Sequence stratigraphy and inferred relative sea-level change from the onshore British Jurassic
title Sequence stratigraphy and inferred relative sea-level change from the onshore British Jurassic
title_full Sequence stratigraphy and inferred relative sea-level change from the onshore British Jurassic
title_fullStr Sequence stratigraphy and inferred relative sea-level change from the onshore British Jurassic
title_full_unstemmed Sequence stratigraphy and inferred relative sea-level change from the onshore British Jurassic
title_short Sequence stratigraphy and inferred relative sea-level change from the onshore British Jurassic
title_sort sequence stratigraphy and inferred relative sea level change from the onshore british jurassic
work_keys_str_mv AT hesselbos sequencestratigraphyandinferredrelativesealevelchangefromtheonshorebritishjurassic